Effects of irrigation and soil management for fodder crops on root zone conditions in a red-brown earth

Soil Research ◽  
1984 ◽  
Vol 22 (2) ◽  
pp. 207 ◽  
Author(s):  
WK Mason ◽  
DR Small ◽  
KE Pritchard

The irrigated red-brown earths in northern Victoria have traditionally been considered unsuitable for intensive cropping owing to unstable soil structure. This experiment was established to determine whether management systems for continuous double cropping or crop/lucerne rotations could be developed for these soils. A range of tillage levels, flood or furrow irrigation treatments and organic matter additions were imposed in December 1981. Soil strength, measured with a field penetrometer, has been significantly reduced by both surface soil management and deep ripping. The stability of surface soil aggregates has been significantly increased by reducing tillage, by avoiding the rapid wetting associated with flood irrigation and by the addition of organic matter. However, there has been no increase in rooting depth or activity of maize crops, as indicated by soil water extraction patterns and midday leaf water potential data, in response to the treatments imposed. However, lucerne rapidly developed an active root system, deeper in the profile than maize. This deeper root system increased the soil water supply for lucerne by approximately 50 mm.

2021 ◽  
Author(s):  
Joann Whalen

Abstract Horticulture involves growing crops and ornamental plants in indoor and outdoor environments. Horticultural crops include food crops such as vegetables and fruits (including tree fruits, small fruits and grapes), as well as nut- and seed-bearing plants, herbs and spices. Many non-food crops are also managed by horticulturalists, including medicinal plants, tobacco, hemp, ornamental plants and flowers. Horticultural crops grow naturally in temperate, sub-tropical and tropical climates of the world, although many of these crops are sufficiently robust that they can be grown in any suitable controlled environment. In 2015, astronauts on the International Space Station grew, harvested and ate red romaine lettuce from their VEGGIE system (Vegetable Production System), which has successfully produced lettuce, Swiss chard, radishes, Chinese cabbage and peas in simulated space environments. The VEGGIE is equipped with adequate lighting, water and nutrients to grow vegetables, relying on the space station's cabin environment for temperature and pressure control, and as a source of carbon dioxide for plant growth (NASA, 2016). Most horticultural crops are planted in soil, although modern cultivation techniques include other media, such as peat-based soil, compost, and inert substrates such as rockwool. A suitable growing media must provide anchorage and stability for the plant roots, considering the diverse life histories of horticultural crops. For example, plants that complete their life cycle in one (annual) or two (biennial) growing seasons does not produce the extensive, deep root system of a woody perennial that lives for several decades. Without adequate anchorage, shrubs and trees are vulnerable to blow down in wind-storms if their roots are in loose, fluid soils or if the plant has a shallow root system on a rocky strata close to the surface. Wind rocking of a poorly-anchored seedling can lead to fine roots breakage and root system detachment from soil, causing the plant to tilt. Soil management refers to the way that soils are cultivated to support horticultural crop growth. Actively growing roots need oxygen for their metabolic function, so the soil must have a crumbly, porous structure that allows for gas exchange with the atmosphere. The porous soil structure permits oxygen diffusion to the root zone, and for carbon dioxide respired by the roots to leave the soil environment. Since plants roots are responsible for obtaining most of the water required for metabolic functions and cooling leaf surfaces, the soil must retain and supply water to the roots while avoiding waterlogging, which inhibits root functions. Soil also provides many essential plant nutrients for crop growth, such as nitrogen, phosphorus, potassium, calcium, magnesium, sulfur and micronutrients (boron, iron, copper, manganese, zinc, chloride, molybdenum and nickel). Nutrient uptake in the root system is facilitated by plant interactions with soil-dwelling microorganisms, both free-living and symbiotic, which are abundant in the root zone. Good soil management is essential to produce nutritious, high yielding food and to support the growth of non-food crops like herbaceous and woody ornamentals. Soil management specialists are responsible for maintaining the soil physical integrity, its chemical balance and soil microbial life necessary for growing horticultural crops.


2008 ◽  
Vol 12 (6) ◽  
pp. 1323-1337 ◽  
Author(s):  
C. Albergel ◽  
C. Rüdiger ◽  
T. Pellarin ◽  
J.-C. Calvet ◽  
N. Fritz ◽  
...  

Abstract. A long term data acquisition effort of profile soil moisture is under way in southwestern France at 13 automated weather stations. This ground network was developed in order to validate remote sensing and model soil moisture estimates. In this paper, both those in situ observations and a synthetic data set covering continental France are used to test a simple method to retrieve root zone soil moisture from a time series of surface soil moisture information. A recursive exponential filter equation using a time constant, T, is used to compute a soil water index. The Nash and Sutcliff coefficient is used as a criterion to optimise the T parameter for each ground station and for each model pixel of the synthetic data set. In general, the soil water indices derived from the surface soil moisture observations and simulations agree well with the reference root-zone soil moisture. Overall, the results show the potential of the exponential filter equation and of its recursive formulation to derive a soil water index from surface soil moisture estimates. This paper further investigates the correlation of the time scale parameter T with soil properties and climate conditions. While no significant relationship could be determined between T and the main soil properties (clay and sand fractions, bulk density and organic matter content), the modelled spatial variability and the observed inter-annual variability of T suggest that a weak climate effect may exist.


2021 ◽  
Author(s):  
Yao Zhang ◽  
Jocelyn M. Lavallee ◽  
Andy D. Robertson ◽  
Rebecca Even ◽  
Stephen M. Ogle ◽  
...  

Abstract. For decades, predominant soil biogeochemical models have used conceptual soil organic matter (SOM) pools and only simulated them to a shallow depth in soil. Efforts to overcome these limitations have prompted the development of new generation SOM models, including MEMS 1.0, which represents measurable biophysical SOM fractions, over the entire root zone, and embodies recent understanding of the processes that govern SOM dynamics. Here we present the result of continued development of the MEMS model, version 2.0. MEMS 2.0 is a full ecosystem model with modules simulating plant growth with above and below-ground inputs, soil water, and temperature by layer, decomposition of plant inputs and SOM, and mineralization and immobilization of nitrogen (N). The model simulates two commonly measured SOM pools – particulate and mineral-associated organic matter (POM and MAOM), respectively. We present results of calibration and validation of the model with several grassland sites in the U.S. MEMS 2.0 generally captured the soil carbon (C) stocks (R2 of 0.89 and 0.6 for calibration and validation, respectively) and their distributions between POM and MAOM throughout the entire soil profile. The simulated soil N matches measurements but with lower accuracy (R2 of 0.73 and 0.31 for calibration and validation of total N in SOM, respectively) than for soil C. Simulated soil water and temperature were compared with measurements and the accuracy is comparable to the other commonly used models. The seasonal variation in gross primary production (GPP; R2 = 0.83), ecosystem respiration (ER; R2 = 0.89), net ecosystem exchange (NEE; R2 = 0.67), and evapotranspiration (ET; R2 = 0.71) were well captured by the model. We will further develop the model to represent forest and agricultural systems and improve it to incorporate new understanding of SOM decomposition.


2010 ◽  
Vol 5 (No. 2) ◽  
pp. 58-68
Author(s):  
S. Kužel ◽  
L. Kolář ◽  
J. Gergel ◽  
J. Peterka ◽  
J. Borová-Batt

: In average samples of three sandy-loamy acid Cambisols from a South Bohemian area labile organic matters were determined by the permangate method modified by the dichromate method, and the rate constant of their biochemical oxidation was determined in hot water extracts of the samples. The need of liming was determined by means of 2 methods. In soil solutions of these samples, all values necessary to evaluate their calcium carbonate equilibriums were determined. The soil samples were enriched with 3% of dry matter of two organic materials, farmyard manure and meadow clover meal, and were incubated at 25&deg;C for 180 days under wetting above 50% of their retention water capacity, and after this procedure all analyses were repeated. Both methods were found to increase the need of liming in all three soils: the more labile the organic matter in 3% addition, the higher the need. The meadow clover matter was more labile than the farmyard manure matter. All three methods for the study of soil carbon lability yielded similar results while the potassium permanganate method was more sensitive than the dichromate one. Increases were observed in equilibrium [Cr(H<sub>2</sub>CO<sub>3</sub>* )] and in Langelier saturation index I<sub>s</sub>. This means that soil liming cannot be considered only as an adjustment to the soil acidity and supply of calcium to plants to meet their requirements, but also as a replacement of the spontaneous adjustment to calcium carbonate equilibrium of soil water, for which through mineralisation of labile organic matters in conditions of our experiment about 220 kg CaCO<sub>3</sub> per hectare of land were consumed on condition that it was not necessary to re-establish it. The process of Ca-compound consumption to establish the calcium carbonate equilibrium is controlled exclusively by the degree of mineralising organic matters lability while the influence of soil properties is only marginal. The same results were provided by the comparison of calcium carbonate equilibriums in nine &Scaron;umava brooks of the total watershed area 78 564 km<sup>2</sup> with the degree of lability of organic matters in their sediments in 1986, 2001 and 2004. A reduction in the intensity of agricultural production in 1986&ndash;2004 resulted in an increase in the stability of organic matters in the sediments, in a decrease in I<sub>s</sub>, and in a lower corrosivity of brooks water towards CaCO<sup>3</sup>. However, the quality of soils and their potential soil fertility decreased due to the loss of labile organic matters.


2013 ◽  
Vol 7 (1) ◽  
pp. 59-68 ◽  
Author(s):  
Zhao Lixi ◽  
Shui Pengbo ◽  
Jiang Fang ◽  
Qiu Hengqing ◽  
Ren Shumei ◽  
...  

2016 ◽  
Author(s):  
F. Büks ◽  
M. Kaupenjohann

Abstract. The stability of soil aggregates against shear and compressive forces as well as water caused dispersion is an integral marker of soil quality. High stability results in less soil compactibility and erodibility, enhanced water retention, a dynamic water transport and aeration regime, increased rooting depth and protection of soil organic matter (SOM) against microbial degradation. For decades the importance of biofilm extracellular polymeric substances (EPS) regarding aggregate stability has been canonical because of its distribution, geometric structure and ability to link primary particles. However, experimental proof is still missing. This lack is mainly due to methodological reasons. Thus, the objective of this work is to develop a method of enzymatic biofilm detachment for studying the effects of EPS on soil aggregate stability. The method combines an enzymatic pre-treatment with different activities of α-glucosidase, β-galactosidase, DNAse and lipase, which preserves aggregate structure, with a subsequent sequential ultrasonic treatment for disaggregation and density-fractioning. Soil organic carbon (SOC) releases of treated samples were compared to an enzyme-free control. To test the effectivity of biofilm detachment the ratio of bacterial DNA from sessile and suspended cells after enzymatic treatment was measured by quantitative real-time PCR. Although the enzyme treatment was not sufficient for total biofilm removal, our results confirm, that EPS stabilizes soil aggregates predominantly by a strong intra-aggregate fixation, and enzymatic biofilm digestion caused a shift of occluded particulate organic matter (POM) to more fragile binding patterns. This suggests that an effect of agricultural practices on soil microbial populations could influence aggregate stability and thereby soil quality.


1969 ◽  
Vol 53 (1) ◽  
pp. 57-60
Author(s):  
M. A. Lugo López ◽  
Raúl Pérez Escolar

A mathematical approach is presented in this paper to evaluate the influence of such factors as clay content, silt content, organic matter, Ca + Mg, and soluble sodium upon the stability of soil aggregates in a group of Vertisols from the Lajas Valley, P.R. The relationships between aggregate stability and silt and clay were not significant. When the percentage of organic matter was considered as the independent variable, a highly significant correlation coefficient of 0.66 was obtained. Therefore, almost 43 percent of the variability in aggregate stability could be explained on the basis of this single factor. Attempts to increase the percentage of the variability which could be explained in terms of the content of Ca + Mg, and also of soluble sodium, yielded correlation coefficients of 0.70 and 0.74, respectively. Thus, only a slight, but significant, additional increase could be explained when these variables were included.


HortScience ◽  
1998 ◽  
Vol 33 (3) ◽  
pp. 553f-554
Author(s):  
A.K. Alva ◽  
A. Fares

Supplemental irrigation is often necessary for high economic returns for most cropping conditions even in humid areas. As irrigation costs continue to increase more efforts should be exerted to minimize these costs. Real time estimation and/or measurement of available soil water content in the crop root zone is one of the several methods used to help growers in making the right decision regarding timing and quantity of irrigation. The gravimetric method of soil water content determination is laborious and doesn't suite for frequent sampling from the same location because it requires destructive soil sampling. Tensiometers, which measure soil water potential that can be converted into soil water content using soil moisture release curves, have been used for irrigation scheduling. However, in extreme sandy soils the working interval of tensiometer is reduced, hence it may be difficult to detect small changes in soil moisture content. Capacitance probes which operate on the principle of apparent dielectric constant of the soil-water-air mixture are extremely sensitive to small changes in the soil water content at short time intervals. These probes can be placed at various depths within and below the effective rooting depth for a real time monitoring of the water content. Based on this continuous monitoring of the soil water content, irrigation is scheduled to replenish the water deficit within the rooting depth while leaching below the root zone is minimized. These are important management practices aimed to increase irrigation efficiency, and nutrient uptake efficiency for optimal crop production, while minimizing the impact of agricultural non-point source pollutants on the groundwater quality.


Soil Research ◽  
1997 ◽  
Vol 35 (4) ◽  
pp. 843 ◽  
Author(s):  
Damien J. Field ◽  
David C. McKenzie ◽  
Anthony J. Koppi

The stability in water of soil from 3 contrasting Vertisols was measured using5 tests. Two end-over-end shaking procedures, the Loveday & Pyledispersion test, and the relatively rapid SOILpak procedure of Daniells & Larsen were assessed. The latter method has been modified to deal with severaldeficiencies such as its lack of score subdivisions; the new procedure isreferred to as the ‘aggregate stability in water’ (ASWAT) test. Wecorrelated data from all the tests under consideration to provide definitionsof the ‘critical’ point at which dispersion becomes a problem forland managers. Three soil management zones have been defined provisionallyusing data from the ASWAT and end-over-end ‘aggregate stability’tests. The scheme allows appropriate surface soil management strategies to bepredicted using the ASWAT test. The relationship between data from the ASWATtest and exchangeable sodium percentage indicated that factors other thanexchangeable sodium strongly influence dispersibility of the samples underconsideration.


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